This is a very qualitative model of the upper layers of the ocean that allows learners to experiment with energy transfer mechanisms.
The temperatures shown have no units and only indicate a relative energy scale.
The ocean water column is assumed to be incompressible, stably stratified by temperature differences, homogeneous with no advection.
The graphic interface shows layers of the ocean water, color coded for temperature (energy content).
To the right of each layer is a number giving the computed temperature of each layer. Values with an asterisk (*)
are part of the ocean isothermal mixed layer. Above these values in the same column, is an overall average of the layer
temperatures.
The important model controls are:
- SOLAR ENERGY
- This control adjusts the solar intensity from LOW to HIGH. OFF turns off the sun.
- HEAT TRANSFER
- Energy transfers happen between the sea and the air. These energy transfers happen by
evaporation, sensible heat and longwave radiation. These transfers are
affected by the air temperature setting (a cool atmosphere absorbs heat from a warm ocean and
visa-versa). These mechanisms are very important for energy balancing.
This control adjusts the heat transfer from LOW to HIGH. OFF turns off the mechanisms.
- WATER TRANSPARENCY
- This control determines how far sunlight energy penetrates below
the surface of the water.
This control adjusts the water transparency/clarity from LOW to HIGH. OFF makes the water very opaque.
- WIND SPEED
- Wind caused turbulence that mixes water inthe surface layers.
This control adjusts the wind speed from LOW to HIGH. OFF turns off the wind.
- WATER DIFFUSION
- Water undergoes diffusion (spread of water molecules) and conduction
(energy transfer between water molecules) that tend to equalize temperatures in
the layers.
This control adjusts diffusion/conduction from LOW to HIGH. OFF turns off the mechanisms.
- AIR TEMPERATURE
- This control sets the air temperature above the ocean. This determines
the temperature threshold that affects whether heat transfers from ocean to
atmosphere or visa-versa.
This control adjusts the air temperature from LOW to HIGH. OFF sets the air temperature to zero.
- INITIAL SURFACE TEMPERATURE
- Use this control to set a starting profile of ocean layer temperatures.
This control adjusts the surface temperature from 0 to 14.
- STEP
- This button runs the model for a fixed time interval.
- CYCLE
- This button runs the model through a solar cycle Winter-Spring-Summer-Fall.
- RESET
- This button resets the model layers to the starting temperature state.
References
- Warren, B. A. (1972), Insensitivity of Subtropical Mode Water Charateristics to Meteorological Fluctuations,
Deep-Sea Research, Vol 19, 1-19.
- Kraus E. B., J. S. Turner (1967), A One-Dimensional Model of the Seasonal Thermocline, II. The General Theory and Its Consequences,
Tellus, 19, 98-105.
- Denman K. L. (1973), A Time-Dependent Model of the Upper Ocean, J. Phys. Oceanogr., 3, 173-184